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河北临城白云洞洞积石形成与风化现象研究
马风书1; 宋林华2; 陈岗岭1; 睢树春1
2000
Source Publication地理学与国土研究
ISSN1001-8107
Volume016Issue:003Pages:68
Abstract发育于中寒武纺厚层状鲕状灰岩和薄层泥质灰岩中的河北临城崆山白云洞是一个上下三层,总长500m、面积4200m^2的小型旅游洞穴。洞内碳酸钙景观极其丰富,其是石幔、卷曲石、石葡萄。白云洞老洞积石发生了强烈的风化,洞积石已变得疏松,易折断和掉块。在老洞积石强烈风化处或在风化洞积石上,发育了新的洞积石。在白云洞所在的崆山山脊上保留了三十万年前形成的大型石笋基群和洞穴石葡萄、石瘤和钙板等。根据洞穴中的裂隙
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/85411
Collection中国科学院地理科学与资源研究所
Affiliation1.河北省临城县旅游局
2.中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714
马风书,宋林华,陈岗岭,等. 河北临城白云洞洞积石形成与风化现象研究[J]. 地理学与国土研究,2000,016(003):68.
APA 马风书,宋林华,陈岗岭,&睢树春.(2000).河北临城白云洞洞积石形成与风化现象研究.地理学与国土研究,016(003),68.
MLA 马风书,et al."河北临城白云洞洞积石形成与风化现象研究".地理学与国土研究 016.003(2000):68.
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